Grain boundary sliding
id:
grain-boundary-sliding-321-12352660
title:
Grain boundary sliding
text:
Grain boundary sliding (GBS) is a material deformation mechanism where grains slide against each other. This occurs in polycrystalline material under external stress at high homologous temperature and low strain rate and is intertwined with creep. Homologous temperature describes the operating temperature relative to the melting temperature of the material. There are mainly two types of grain boundary sliding: Rachinger sliding, and Lifshitz sliding. Grain boundary sliding usually occurs as a co
brand slug:
wiki
category slug:
encyclopedia
description:
Material deformation mechanism
original url:
https://en.wikipedia.org/wiki/Grain_boundary_sliding
date created:
date modified:
2024-02-09T09:11:10Z
main entity:
{"identifier":"Q2653922","url":"https://www.wikidata.org/entity/Q2653922"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/f/f1/GBsliding.tif","width":3000,"height":1688}
fields total:
13
integrity:
15